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Figure 2 Method for calculating the estimated groundwater flux.
Silica concentration is dependent on the relative proportion of local (shallow) and regional (deep) groundwater flux.
The groundwater flux from area Y differs from the entire aquifer's (X) flux.
The average groundwater flux in our data is 303 m3/day (Table 1).
These tracers are displaced from the sorbent at rates proportional to the groundwater flux; hence, in the current meter design, the resident tracers are used to quantify cumulative groundwater flux.
Temperature-based methods were used to estimate the groundwater flux distribution.
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Correlations between prediction uncertainties for lithofacies, hydraulic heads and groundwater fluxes were also investigated.
The successful management of groundwater dependent shallow seasonal wetlands requires a sound understanding of groundwater fluxes.
In most regions, information on groundwater fluxes and surface outflows are not available because gauging networks are absent.
Shallow groundwater fluxes to/from the pond were controlled by water storage in and exchange with the adjacent riparian peatlands.
Shallow groundwater fluxes may have contributed as much as 23% of inputs and outputs, and influenced pond chemistry and permanence.
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